1 Jet Propulsion Laboratory, California Institute of Technology , Pasadena, California.
2 The Robotics Institute, Carnegie Mellon University , Pittsburgh, Pennsylvania.
Astrobiology. 2018 Jul;18(7):934-954. doi: 10.1089/ast.2017.1782.
Ancient hydrothermal systems are a high-priority target for a future Mars sample return mission because they contain energy sources for microbes and can preserve organic materials (Farmer, 2000 ; MEPAG Next Decade Science Analysis Group, 2008 ; McLennan et al., 2012 ; Michalski et al., 2017 ). Characterizing these large, heterogeneous systems with a remote explorer is difficult due to communications bandwidth and latency; such a mission will require significant advances in spacecraft autonomy. Science autonomy uses intelligent sensor platforms that analyze data in real-time, setting measurement and downlink priorities to provide the best information toward investigation goals. Such automation must relate abstract science hypotheses to the measurable quantities available to the robot. This study captures these relationships by formalizing traditional "science traceability matrices" into probabilistic models. This permits experimental design techniques to optimize future measurements and maximize information value toward the investigation objectives, directing remote explorers that respond appropriately to new data. Such models are a rich new language for commanding informed robotic decision making in physically grounded terms. We apply these models to quantify the information content of different rover traverses providing profiling spectroscopy of Cuprite Hills, Nevada. We also develop two methods of representing spatial correlations using human-defined maps and remote sensing data. Model unit classifications are broadly consistent with prior maps of the site's alteration mineralogy, indicating that the model has successfully represented critical spatial and mineralogical relationships at Cuprite. Key Words: Autonomous science-Imaging spectroscopy-Alteration mineralogy-Field geology-Cuprite-AVIRIS-NG-Robotic exploration. Astrobiology 18, 934-954.
古老的热液系统是未来火星样本返回任务的首要目标,因为它们为微生物提供了能源,并能保存有机物质(Farmer,2000;MEPAG 下一个十年科学分析小组,2008;McLennan 等人,2012;Michalski 等人,2017)。由于通信带宽和延迟的原因,用远程探测器来描绘这些大型、非均质系统具有挑战性;这样的任务将需要在航天器自主性方面取得重大进展。科学自主性使用智能传感器平台实时分析数据,为调查目标设置测量和下传优先级,以提供最佳信息。这种自动化必须将抽象的科学假设与机器人可用的可测量量联系起来。本研究通过将传统的“科学可追溯性矩阵”形式化为概率模型来捕捉这些关系。这允许使用实验设计技术来优化未来的测量,最大限度地提高调查目标的信息价值,指导远程探测器对新数据做出适当反应。这种模型是一种新的语言,用于以物理为基础的术语来指挥明智的机器人决策。我们应用这些模型来量化不同漫游车穿越的信息量,对内华达州 Cuprite 山进行了 profiling 光谱分析。我们还开发了两种使用人类定义的地图和遥感数据表示空间相关性的方法。模型单元分类与该地点蚀变矿物学的先前地图广泛一致,表明该模型已成功地代表了 Cuprite 地区关键的空间和矿物学关系。关键词:自主科学-成像光谱学-蚀变矿物学-野外地质-Cuprite-AVIRIS-NG-机器人探索。天体生物学 18,934-954。